Joint 52nd Northeastern Annual Section / 51st North-Central Annual Section Meeting - 2017

Paper No. 5-3
Presentation Time: 8:45 AM

A GEOCHEMICAL CONTEXT FOR STRAY GAS INVESTIGATIONS IN THE N. APPALACHIAN BASIN: IMPLICATIONS OF ANALYSES OF NATURAL GASES FROM NEOGENE-THROUGH-DEVONIAN-AGE STRATA


BALDASSARE, Fred, 1229 Twelve Oaks Ct, Murrysville, PA 15668, MCCAFFREY, Mark, 3141 Hood Street, Suite 103, Dallas, TX 75219 and HARPER, John A., Pennsylvania Geological Survey (ret), 5430 Fredanna St, Pittsburgh, PA 15207, fbaldassare@echelonagc.com

As the pace of drilling activity to the Marcellus Formation in the northern Appalachian Basin increased, so did the number of alleged incidents of stray natural gas migration to shallow aquifer systems.

More than 2,300 gas and water samples were analyzed in the present study for (1) molecular composition, (2) stable carbon and hydrogen isotope compositions of methane and (3) stable carbon isotope composition of ethane. The samples are from Neogene to Middle Devonian-age strata in a five-county study area in northeastern Pennsylvania. Gas and water samples were collected from (1) 234 gas wells during Mudgas Logging (MGL) programs for wells being drilled to the Marcellus Shale Formation, and (2) 67 private water supply wells during baseline groundwater water-quality testing programs. Regional and local geologic conditions were evaluated from core analyses and published studies.

Evaluation of this geochemical database reveals that microbial, mixed microbial/thermogenic, and thermogenic gases occur in some shallow aquifer systems, and that the gas occurrences pre-date Marcellus Formation drilling activity. The isotope data reveal that thermogenic gases in the Neogene and Upper Devonian strata are typically distinct from gases from deeper Middle Devonian strata (including the Marcellus Fm.).

Significantly, however, a more detailed review of the geochemistry at the site-specific level also reveals a complex thermal and migration history with gas mixtures indicated by partial isotope reversals (δ13C113C2) in some areas throughout the stratigraphic section above the Marcellus Formation.

Defining a specific source for stray natural gas requires the investigation and synthesis of several data types at the site-specific level. Evaluation of gas geochemistry data provides evidence of gas origin. Additional investigation to delineate migration pathways and the mechanism of migration are necessary to further constrain and identify specific stray gas source(s). A case study will be presented highlighting the complexity and site specificity of stray gas migration investigations.